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Mechanism of particle granulation in the vibrofluidized bed. / Ryzhko, A. F.; Mikula, V. A.
In: Inzhenerno-Fizicheskii Zhurnal, Vol. 61, No. 1, 1991, p. 112-116.

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Harvard

Ryzhko, AF & Mikula, VA 1991, 'Mechanism of particle granulation in the vibrofluidized bed', Inzhenerno-Fizicheskii Zhurnal, vol. 61, no. 1, pp. 112-116.

APA

Vancouver

Ryzhko AF, Mikula VA. Mechanism of particle granulation in the vibrofluidized bed. Inzhenerno-Fizicheskii Zhurnal. 1991;61(1):112-116.

Author

Ryzhko, A. F. ; Mikula, V. A. / Mechanism of particle granulation in the vibrofluidized bed. In: Inzhenerno-Fizicheskii Zhurnal. 1991 ; Vol. 61, No. 1. pp. 112-116.

BibTeX

@article{d06369f1f2ff4ad48010165048cfdfb0,
title = "Mechanism of particle granulation in the vibrofluidized bed",
abstract = "Simple relations for calculation of unit diameters are proposed from the balance of inertia and autoadhesion forces with regard to the dominating moisture form in units. Calculation results agree well with the data of the present authors and other researchers. The experiments are carried out at the porosity 0.38-0.42. Conclusion is made, that in the moisture interval 0-20% the three characteristic granule sizes exist. This sizes determine by the moisture coupling with material. The granule size dependence on the initial particle size and bed moisture are presented. The mechanisms of granule destruction are analyzed. The vibrofluidization condition is obtained.",
author = "Ryzhko, {A. F.} and Mikula, {V. A.}",
year = "1991",
language = "Русский",
volume = "61",
pages = "112--116",
journal = "Inzhenerno-Fizicheskii Zhurnal",
issn = "0021-0285",
publisher = "Институт тепло- и массообмена им. А.В. Лыкова Национальной академии наук Беларуси",
number = "1",

}

RIS

TY - JOUR

T1 - Mechanism of particle granulation in the vibrofluidized bed

AU - Ryzhko, A. F.

AU - Mikula, V. A.

PY - 1991

Y1 - 1991

N2 - Simple relations for calculation of unit diameters are proposed from the balance of inertia and autoadhesion forces with regard to the dominating moisture form in units. Calculation results agree well with the data of the present authors and other researchers. The experiments are carried out at the porosity 0.38-0.42. Conclusion is made, that in the moisture interval 0-20% the three characteristic granule sizes exist. This sizes determine by the moisture coupling with material. The granule size dependence on the initial particle size and bed moisture are presented. The mechanisms of granule destruction are analyzed. The vibrofluidization condition is obtained.

AB - Simple relations for calculation of unit diameters are proposed from the balance of inertia and autoadhesion forces with regard to the dominating moisture form in units. Calculation results agree well with the data of the present authors and other researchers. The experiments are carried out at the porosity 0.38-0.42. Conclusion is made, that in the moisture interval 0-20% the three characteristic granule sizes exist. This sizes determine by the moisture coupling with material. The granule size dependence on the initial particle size and bed moisture are presented. The mechanisms of granule destruction are analyzed. The vibrofluidization condition is obtained.

UR - http://www.scopus.com/inward/record.url?partnerID=8YFLogxK&scp=0026194530

M3 - Статья

VL - 61

SP - 112

EP - 116

JO - Inzhenerno-Fizicheskii Zhurnal

JF - Inzhenerno-Fizicheskii Zhurnal

SN - 0021-0285

IS - 1

ER -

ID: 54788369